Olivine has a distinctive green color, making it easy to identify visually. It has a high hardness of 6.5-7 on the Mohs scale, aiding in its differentiation from other minerals. Olivine often occurs in tabular or elongate crystal shapes, which can help distinguish it from similar minerals.
Olivine typically exhibits a glassy or vitreous luster. This is due to its composition of magnesium, iron, and silicate minerals, which create a smooth, reflective surface when light interacts with the crystal structure. The luster of olivine can vary depending on the specific composition and crystal structure of the mineral.
Olivine does not contain Gabbro. Gabbro can contain olivine. Usually no more than a few percent.
willemite
Olivine is mined in various countries around the world, including the United States, Norway, Finland, and India. Some of the major olivine mining locations include Hawaii (forsterite-rich olivine), Norway (fayalite-rich olivine), and Finland. These regions have significant deposits of olivine due to their geological history and processes.
Quartz scratches dolomite but is scratched by olivine. Dolomite has a Mohs hardness of 3.5-4, while quartz has a hardness of 7. Olivine, on the other hand, has a higher hardness of 6.5-7.
Olivine is a nonmetallic mineral with a hardness on the Mohs Hardness Scale of 7. It has a white streak and its color is pale or dark olive-green to yellow, or brown. It forms short crystals that may resemble sand grains. Also, it has a conchoidal fracture and has no cleavage. It is brittle and has a specific gravity of 3.3 to 3.4.
Olivine has a distinctive green color, making it easy to identify visually. It has a high hardness of 6.5-7 on the Mohs scale, aiding in its differentiation from other minerals. Olivine often occurs in tabular or elongate crystal shapes, which can help distinguish it from similar minerals.
Quartz would be able to scratch fluorite, galena, and pyroxene as it is harder than these minerals on the Mohs scale of hardness.
Olivine typically exhibits a glassy or vitreous luster. This is due to its composition of magnesium, iron, and silicate minerals, which create a smooth, reflective surface when light interacts with the crystal structure. The luster of olivine can vary depending on the specific composition and crystal structure of the mineral.
Olivine fractures.
Its not at the port
Olivine city
four common members of olivine family that is 1) FORSTERITE ((Mg) 2SiO4.2) fayalite(Fe) 2SiO43)olivineMn SiO44) tephorite( Mn2SiO4)
strength is in olivine city in the olivine cafe
you can find olivine rocks in volcanoes in Greenland.
the cafe in olivine is to the LEFT of the poke centre,